Rock Identifier
Petrified Wood (Silicified Wood (Permineralized organic tissue)) — fossil
fossil

Petrified Wood

Silicified Wood (Permineralized organic tissue)

Hardness: 6.5 to 7 on the Mohs scale; Color: Brown, grey, black, red, yellow; Luster: Vitreous to dull; Crystal structure: Microcrystalline quartz (chalcedony/opal); Cleavage: None

Hardness
6
Color
Brown, grey, black, red, yellow
Luster
Vitreous to dull
Identified More fossil
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Physical properties

Hardness: 6.5 to 7 on the Mohs scale; Color: Brown, grey, black, red, yellow; Luster: Vitreous to dull; Crystal structure: Microcrystalline quartz (chalcedony/opal); Cleavage: None

Formation & geological history

Formed when buried wood is slowly replaced by minerals (usually silica, quartz, or opal) over millions of years, often in ancient floodplains or volcanic ash beds during the Mesozoic and Cenozoic eras.

Uses & applications

Used for ornamental objects, polished display specimens, lapidary art, bookends, and jewelry making.

Geological facts

Petrified wood retains the original cellular structure of the tree while turning completely to stone, sometimes preserving tree rings and bark details microscopic in precision.

Field identification & locations

Look for visible wood grain and bark texture combined with a heavy stone weight and glass-like hardness that can scratch glass. Commonly found in deserts, badlands, and regions with ancient volcanic activity.